Urbanization Drives Carbon Dioxide Supersaturation in South Asian River Networks: Insights from the Krishna River Basin, India
ACS ES&T Water,
Journal Year:
2025,
Volume and Issue:
unknown
Published: Feb. 6, 2025
Rivers
are
globally
significant
sources
of
atmospheric
carbon
dioxide
(CO2).
However,
the
processes
governing
supersaturation
CO2
in
large
tropical
fluvial
networks
poorly
understood.
In
particular,
strikingly
little
is
known
about
role
land
use
shaping
variability
South
Asian
river
basins,
which
undergoing
rapid
urbanization.
Here,
we
show
that
wide
partial
pressure
(pCO2:
246.3–21271.2
μatm)
an
agriculture-dominated
basin
(Krishna
River
basin,
India)
primarily
shaped
by
extent
Specifically,
a
strong
positive
correlation
between
pCO2
and
built-up
area
(%)
was
observed
when
exceeded
2%.
Furthermore,
machine
learning
analysis
showed
predicted
(%),
Strahler
order,
altitude,
together
explaining
∼77%
spatial
variability.
Additionally,
negative
excess
oxygen
relative
to
equilibrium
indicates
in-stream
metabolism,
fueled
organic
matter
inputs
from
urbanized
areas,
primary
cause
supersaturation,
establishing
mechanistic
link
area.
Given
increases
with
urbanization,
limiting
urban
crucial
for
reducing
emissions
basins.
Language: Английский
Diverse Altitudinal Patterns and Drivers of Greenhouse Gas Dynamics in Southwest China Alpine Streams and Rivers
Ying Wang,
No information about this author
Yuhao Li,
No information about this author
Genxu Wang
No information about this author
et al.
Journal of Geophysical Research Biogeosciences,
Journal Year:
2025,
Volume and Issue:
130(2)
Published: Feb. 1, 2025
Abstract
Streams
and
rivers
are
globally
significant
sources
of
greenhouse
gases
(GHGs)
to
the
atmosphere.
However,
GHG
evasion
from
mountain
streams
remains
poorly
constrained
due
scarce
data.
In
this
study,
we
measured
concentrations
estimated
fluxes
riverine
carbon
dioxide
(CO
2
),
methane
(CH
4
nitrous
oxide
(N
O)
across
three
alpine
catchments
in
Southwest
China.
these
turbulent
slightly
oversaturated
but
much
lower
than
global
average,
likely
high
gas
transfer
velocities
that
rapidly
deplete
GHGs.
Headwater
(first‐order)
exhibited
higher
rates
large
(fourth‐order),
despite
having
CO
N
O
concentrations.
The
partial
pressure
dissolved
decreased
linearly
with
elevation,
linked
altitudinal
patterns
forest
cover
groundwater
table
depth.
Dissolved
CH
GHGs
showed
weak
relationships
elevation.
We
observed
seasonal
differences
fluxes,
during
wet
season.
spatial
heterogeneity
stream
was
primarily
controlled
by
hydrology,
climate,
geomorphology.
Our
analyses
also
revealed
were
positively
correlated
water
temperature,
velocity,
channel
slope.
This
study
demonstrates
underestimated
net
GHGs,
particularly
O,
highlighting
importance
headwater
systems
regional
budgets.
diverse
dynamics
suggest
complex
controls
rivers.
Language: Английский
CH4 and CO2 emissions and dissolved carbon exporting in rivers on the upper Lanzhou section of the Yellow River, China
Zhiheng Du,
No information about this author
Hao Cui,
No information about this author
Fangping Yan
No information about this author
et al.
Geoscience Frontiers,
Journal Year:
2025,
Volume and Issue:
unknown, P. 102057 - 102057
Published: April 1, 2025
Language: Английский
The spatial–temporal variability of methane emissions in a montane headstream: implication of precipitation, morphology and microhabitat
Journal of Hydrology,
Journal Year:
2025,
Volume and Issue:
unknown, P. 133534 - 133534
Published: May 1, 2025
Language: Английский
Anthropogenic Perturbations Complicated the Downstream Greenhouse Gas Dynamics of a Large Subtropical Reservoir
Xiang Wan,
No information about this author
Shuai Chen,
No information about this author
Wanfa Wang
No information about this author
et al.
Journal of Geophysical Research Biogeosciences,
Journal Year:
2024,
Volume and Issue:
129(12)
Published: Dec. 1, 2024
Abstract
River
damming
can
significantly
alter
the
hydrology
and
nutrient
levels
of
river
water,
resulting
in
substantial
greenhouse
gas
(GHG)
emissions
to
atmosphere.
However,
dynamics
gases
discharged
water
downstream
dams
remain
poorly
understood,
despite
being
recognized
as
a
crucial
source
GHG
river‐reservoir
systems.
In
this
study,
we
conducted
comprehensive
measurements
concentrations
chemistry
large
subtropical
reservoir
its
upstream
rivers
investigate
spatiotemporal
patterns
fluxes
identify
their
governing
mechanisms,
with
primary
focus
on
dynamics.
Our
analysis
revealed
that
distribution
p
CO
2
among
was
predominantly
controlled
by
aquatic
metabolism
atmospheric
exchange.
Conversely,
CH
4
N
O
largely
influenced
anaerobic
metabolism.
Seasonal
fluctuations
were
linked
hydroclimatic
conditions,
including
temperature,
hydrologic
connectivity
between
land
rivers,
thermal
stratification.
Anthropogenic
activities
(e.g.,
agricultural
use)
found
affect
trend
concentrations.
Higher
compared
attributed
production
increased
transfer
velocity
rivers.
These
findings
underscore
critical
influence
anthropogenic
emphasize
necessity
integrating
impacts
seasonal
variability
enhance
our
understanding
carbon
budget
Language: Английский
Anthropogenic and Hydroclimatic Controls on the CO2 and CH4 Dynamics in Subtropical Monsoon Rivers
Shuai Chen,
No information about this author
Lishan Ran,
No information about this author
Clément Duvert
No information about this author
et al.
Water Resources Research,
Journal Year:
2024,
Volume and Issue:
61(1)
Published: Dec. 27, 2024
Abstract
Anthropogenic
perturbations
have
substantially
altered
riverine
carbon
cycling
worldwide,
exerting
influences
on
dissolved
dioxide
(CO
2
)
and
methane
(CH
4
dynamics
at
multiple
levels.
However,
the
magnitude
role
of
anthropogenic
activities
in
modulating
emissions
across
entire
river
networks,
as
well
influence
climatic
controls,
remain
largely
unresolved.
Here,
we
explore
controlling
factors
CO
CH
62
subtropical,
monsoon‐influenced
streams
rivers
through
basin‐wide
seasonal
measurements.
We
found
that
land
use
aquatic
metabolism
played
significant
roles
regulating
spatial
temporal
patterns
both
gases.
Increased
nutrient
levels
organic
matter
contributed
to
higher
partial
pressure
(
p
).
Dissolved
oxygen,
stable
isotope
inorganic
carbon,
proportion
impervious
surface,
catchment
slope,
width
were
major
predictors
for
.
For
,
Chlorophyll
a
water
temperature,
which
availability
methanogenesis.
Seasonal
variations
strongly
modulated
by
hydroclimatic
conditions,
with
temperature
markedly
ecosystem
metabolism.
These
findings
highlight
likelihood
changes
climate
evolve,
thereby
profoundly
affecting
global
cycle.
Language: Английский